“…The similar slopes between our study and those reported by Grigal (2002) for the THg DOC relationship are likely a function of strong correlation between FTHg and the export of humic material associated with hydrophobic organic matter (Mierle and Ingram, 1991;Grigal, 2002).…”
Section: Ajessupporting
confidence: 90%
“…AJES previous studies showed a strong interactions between Hg and DOM have also been indicated by a positive correlation between their concentrations in many natural waters (Andren and Harriss, 1975;Lindberg and Harriss, 1974;Mierle and Ingram, 1991;Meili et al, 1991;Driscoll et al, 1995;Hurley et al, 1995;Watras et al, 1995;Baeyens et al, 1996;Kolka et al, 1999;Shanley et al, 2002).…”
This study addresses the correlations between Hg and organic matter in recent sediment; samples were collected from the Gulf of Aqaba, Red Sea coasts (oligotrophic regions) during 2010. In the present study TOC analyzer was used to determine Total Organic Carbon (TOC) and Total Nitrogen (TN) concentrations and the total amount of mercury (Hg T ) in sediment samples were analyzed by Hydra-C mercury analyzer. The obtained results indicated that, mercury, TOC and TN average concentrations in the Red Sea were 85.42 ng g −1 , 5.10 and 4.45 mg L −1 , respectively. The results show that the Total Organic Carbon (TOC) in sediment represents the sum of various organic compounds, which may play a completely different role in the distribution and accumulation of Hg. slightly correlations between the TOC and the concentration of Hg in the studied sediment arise mainly from the labile portion of organic matter released. These compounds primarily consist of easily degradable algal-derived lipids and various pigments, which are petrographically described as a soluble Organic Matter (OM). The preserved OM in sediment is commonly entrapped within the cell walls of phytoplankton and also appears as a surface coating on sediment particles. The strong affinity between Hg and OM is due not only to its chemical reactivity, but also to the physical characteristic of these labile compounds, which plays the most important role in the distribution of Hg in sediment.
“…The similar slopes between our study and those reported by Grigal (2002) for the THg DOC relationship are likely a function of strong correlation between FTHg and the export of humic material associated with hydrophobic organic matter (Mierle and Ingram, 1991;Grigal, 2002).…”
Section: Ajessupporting
confidence: 90%
“…AJES previous studies showed a strong interactions between Hg and DOM have also been indicated by a positive correlation between their concentrations in many natural waters (Andren and Harriss, 1975;Lindberg and Harriss, 1974;Mierle and Ingram, 1991;Meili et al, 1991;Driscoll et al, 1995;Hurley et al, 1995;Watras et al, 1995;Baeyens et al, 1996;Kolka et al, 1999;Shanley et al, 2002).…”
This study addresses the correlations between Hg and organic matter in recent sediment; samples were collected from the Gulf of Aqaba, Red Sea coasts (oligotrophic regions) during 2010. In the present study TOC analyzer was used to determine Total Organic Carbon (TOC) and Total Nitrogen (TN) concentrations and the total amount of mercury (Hg T ) in sediment samples were analyzed by Hydra-C mercury analyzer. The obtained results indicated that, mercury, TOC and TN average concentrations in the Red Sea were 85.42 ng g −1 , 5.10 and 4.45 mg L −1 , respectively. The results show that the Total Organic Carbon (TOC) in sediment represents the sum of various organic compounds, which may play a completely different role in the distribution and accumulation of Hg. slightly correlations between the TOC and the concentration of Hg in the studied sediment arise mainly from the labile portion of organic matter released. These compounds primarily consist of easily degradable algal-derived lipids and various pigments, which are petrographically described as a soluble Organic Matter (OM). The preserved OM in sediment is commonly entrapped within the cell walls of phytoplankton and also appears as a surface coating on sediment particles. The strong affinity between Hg and OM is due not only to its chemical reactivity, but also to the physical characteristic of these labile compounds, which plays the most important role in the distribution of Hg in sediment.
“…The strong association of Hg and organic matter in surface waters has long been recognized (Lindberg and Harriss 1974;Mierle and Ingram 1991), and numerous studies of Hg in streams and lakes of mid-and northern latitudes of the northern hemisphere have generally shown strong correlations between dissolved Hg concentrations and dissolved organic carbon (DOC) concentrations, and between particulate Hg concentrations and particulate organic carbon concentrations (POC) (Grigal 2002;Yin and Balogh 2002;Dennis et al 2005;Brigham et al 2009;Riscassi and Scanlon 2011). The association of Hg with organic matter is sufficiently strong in many surface waters, that measures such as DOC or absorbance at 254 nm (UV 254 ) have been suggested as surrogates for Hg concentrations, because Hg analyses are expensive and may be unstable in automated water samplers (Dittman et al 2009).…”
Section: Introductionmentioning
confidence: 99%
“…Thus, the association of Hg with the aromatic fraction of organic matter may be rooted in the complex chemistry of Hg interactions with natural organic matter. In addition to geochemistry-based reasons why Hg is more strongly associated with aromatic organic matter, this association may also originate through mobilization to surface waters and mixing of Hg and DOM from principal runoff source areas such as humic-rich shallow soils (Dittman et al 2010) as well as riparian wetland soils (Å gren et al 2008;Mierle and Ingram 1991), two locations where preferential storage of Hg has been identified (Grigal 2003). In summary, Hg-DOM chemistry, storage, and hydrology are interrelated in complex ways that are the subject of ongoing research; thus, determining the primacy of any single explanation for an association that is evident at the basin scale may be difficult.…”
FTHg and SUVA 254 that are characteristic of source areas that control the mobilization of Hg to surface waters, and that the seasonal influence of these source areas varies in this heterogeneous basin landscape.
“…One of the most important reactions is the formation of extremely strong ionic bonding between mercury and reduced sulphur sites in soil and aquatic organic matter. Strong complexation facilitates the mobility of mercury from natural and contaminated soils and sediments 47 into streams, 48 lakes, 49 and groundwater. 50 This enhanced mobility results in increased water column concentrations of mercury in otherwise pristine lakes and streams.…”
Metilmercúrio (MeHg) e mercúrio total (Hg) foram determinados em amostras de água e peixe coletadas em dois reservatórios da Amazônia Brasileira, que apresentam diferentes características limnológicas e ecológicas. As amostras de água de Tucuruí, reservatório mesotrófico com águas claras, apresentaram a concentração de Hg (12,7 ± 8,4 ng L ), an oligotrophic reservoir with black water. Neither Cichla spp. (piscivorous fish), nor Geophagus surinamensis (omnivorous fish) presented significant differences in length-normalized concentrations of MeHg and Hg in muscle, between both reservoirs. MeHg and Hg increased with body weight and standard length of Cichla spp., and also with the trophic level on the food chain. The Hg bioconcentration factor (BCF) increased with the trophic level of the fish, from the omnivorous (10 3 ) to piscivorous fish (10 4 ). Fish from Balbina, an ecosystem naturally rich in dissolved organic matter, presented the highest BCF. Not only the different limnological and ecological characteristics but also the feeding habits seem to influence the mercury concentration in fish.
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